Institute of Nuclear Physics, Polish Academy of Sciences, Radzikowskiego 152, 31-342 Cracow, Poland.
J Phys Condens Matter. 2010 Apr 14;22(14):145402. doi: 10.1088/0953-8984/22/14/145402. Epub 2010 Mar 19.
The structure and stability properties of wadsleyite II as the new phase of Mg(2)SiO(4) has been studied at high pressure by the DFT method. The pressure range corresponds to the transition zone in the Earth. At zero pressure the calculated lattice parameters of the wadsleyite II structure are a=5.749 Å, b=28.791 Å and c=8.289 Å with the density ρ=3406 kg m(-3). The third order Birch-Murnaghan equation of state has been determined for the structure with isothermal bulk moduli K(T)=160.1 GPa and K(T)'=4.3 at a pressure range up to 50 GPa. The elasticity tensor coefficients C(ij)(P), as well as the compressional and shear wave velocities and their pressure derivatives, have been calculated using the deformation method at a range of pressures up to 25 GPa. The results agree with the experimental data and structure properties of the wadsleyite II model. The properties of the wadsleyite II phase are very close to the wadsleyite phase.
用 DFT 方法研究了作为 Mg(2)SiO(4)新相的尖晶石 II 的结构和稳定性特性。压力范围对应于地球的过渡带。在零压力下,尖晶石 II 结构的计算晶格参数为 a=5.749 Å, b=28.791 Å 和 c=8.289 Å,密度 ρ=3406 kg m(-3)。已经确定了结构的三阶 Birch-Murnaghan 状态方程,等温体弹性模量 K(T)=160.1 GPa 和 K(T)'=4.3,压力范围高达 50 GPa。在高达 25 GPa 的压力范围内,使用变形法计算了弹性张量系数 C(ij)(P),以及压缩波和剪切波速度及其压力导数。结果与实验数据和尖晶石 II 模型的结构特性一致。尖晶石 II 相的性质与尖晶石相非常接近。